樱岛昭和火山口火山爆发前的过程(<专题>樱岛特刊)

A. Yokoo, M. Iguchi, Takeshi Tameguri, Keigo Yamamoto
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引用次数: 35

摘要

静止58年的樱岛火山昭和火山口在2006年6月重新活跃起来。从多参数地球物理观测中,我们已经确定了通常发生在火山口爆发之前的过程。在喷发前几小时,岩浆开始迁移并在大约1公里的深度积聚。这种岩浆的聚集可以在应变变化记录中作为膨胀过程清楚地观察到。在喷发前几十分钟,SO2气体排放率逐渐降低,表明随着喷发的临近,火山口底部正在发生封闭过程。在同一时期,火山的膨胀率开始加速,因为在管道上方形成了一个堵塞,防止气体逸出,结果在火山口下方形成了一个气穴。在夜间活动中,也可以看到火山辉光,它减弱然后消失。在火山喷发前几分钟,会有轻微的震动。当储存的气体通过限制气袋的桥塞内的新裂缝释放时,随着应变从膨胀到收缩的变化,其振幅也随之增大,从而导致导管内的轻微降压。然后,一个膨胀过程开始,这可以从地震上解释爆炸地震的第一次运动。这可能是当火山口底部向下的减压作用到达岩浆头时,岩浆突然膨胀并开始脱气。在很短的一段时间(大约半秒)后,膨胀的岩浆上升并推动气袋向上,导致火山口地面随着前一阶段次声波的辐射而膨胀,然后发生破裂。当塞子因变形而失效后,积聚的气体和膨胀的岩浆一起从火山口喷出,地表喷发现象开始。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Processes Prior to Outbursts of Vulcanian Eruption at Showa Crater of Sakurajima Volcano(<Special Section>Sakurajima Special Issue)
Showa crater of Sakurajima volcano became active in June 2006 after 58 years of quiescence. From multiparametric geophysical observations, we have identified the processes that typically occur prior to an explosive eruption at the crater. A few hours prior to the onset of an eruption, magma starts to migrate and accumulates at a depth of about 1 km. This accumulation of magma can be clearly observed in strain change records as an inflation process. Several tens of minutes prior to an eruption, the SO2 gas emission rate gradually decreases, indicating that a sealing process is taking place in the crater bottom as the eruption nears. During the same time period, the volcanoʼs inflation rate starts to accelerate due to the formation of a plug above the conduit that prevents the gas from escaping, with the result that a gas pocket forms beneath the crater. In nighttime events, a volcanic glow is also seen, which weakens and then disappears. A few minutes prior to an eruption, a small tremor starts to occur. Its amplitude grows as the strain changes from inflation to deflation as the stored gas is released through new fractures within the plug that had been confining the gas pocket, leading to a minor depressurization in the conduit. Then, an expansion process starts, that could explain seismically the first motion of an explosion earthquake. This is probably when the effect of depressurization downward from the crater bottom reaches the magma head and a sudden magma expansion with degassing starts. After a short period (about half a second), this expanding magma rises and pushes the gas pocket upward, leading to a swelling of the crater ground along with the radiation of the preceding phase of infrasound waves, and then a breakup occurs. After the plug fails due to deformation, the accumulated gasses and expanding magma are ejected together from the crater as the surface eruption phenomena starts.
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